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Wang, Daming; Van der Voo, Rob; Peacor, Donald R (2005): (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 67-495. PANGAEA,, In supplement to: Wang, D et al. (2005): Why is the remanent magnetic intensity of Cretaceous MORB so much higher than that of mid to late Cenozoic MORB? Geosphere, 1(3), 138-146,

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Latitude: 12.496300 * Longitude: -91.037700
Date/Time Start: 1979-05-26T00:00:00 * Date/Time End: 1979-05-26T00:00:00
Minimum DEPTH, sediment/rock: 428.54 m * Maximum DEPTH, sediment/rock: 441.14 m
67-495 * Latitude: 12.496300 * Longitude: -91.037700 * Date/Time: 1979-05-26T00:00:00 * Elevation: -4140.0 m * Penetration: 455.5 m * Recovery: 333.7 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Device: Drilling/drill rig (DRILL) * Comment: 48 cores; 446 m cored; 9.5 m drilled; 74.8 % recovery
#NameShort NameUnitPrincipal InvestigatorMethodComment
1DEPTH, sediment/rockDepthmGeocode
2AGEAgeka BPGeocode
3Sample code/labelSample labelWang, DamingODP sample designation
4Curie temperatureCurie temp°CWang, Daming
5Hysteresis, saturation magnetization/ saturation remanenceMrs/MsWang, Damingvibrating sample magnetometer (microVSM)
6Hysteresis, coercivity of remanence/coercivityHcr/HcWang, Damingvibrating sample magnetometer (microVSM)
7Hysteresis, saturation remanenceMrsmA m2/kgWang, Damingvibrating sample magnetometer (microVSM)
8CoercivityHcmTWang, Damingvibrating sample magnetometer (microVSM)
9NRM, Intensity per unit massInten (NRM) /mass10-6 A*m2/kgWang, Damingvibrating sample magnetometer (microVSM)
25 data points

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